SLIDE 1 AM 205: lecture 16
◮ Last time: hyperbolic PDEs ◮ Today: parabolic and elliptic PDEs, introduction to
SLIDE 2
The Wave Equation
We now briefly return to the wave equation: utt − c2uxx = 0 In one spatial dimension, this models, say, vibrations in a taut string
SLIDE 3 The Wave Equation
Many schemes have been proposed for the wave equation One good option is to use central difference approximations1 for both utt and uxx: Un+1
j
− 2Un
j + Un−1 j
∆t2 − c2 Un
j+1 − 2Un j + Un j−1
∆x2 = 0 Key points:
◮ Truncation error analysis =
⇒ second-order accurate
◮ Fourier stability analysis =
⇒ stable for 0 ≤ c∆t/∆x ≤ 1
◮ Two-step method in time, need a one-step method to “get
started”
1Can arrive at the same result by discretizing the equivalent first order
system
SLIDE 4
Parabolic PDEs
SLIDE 5 The Heat Equation
The canonical parabolic equation is the heat equation ut − αuxx = f (t, x), where α models thermal diffusivity In this section, we shall omit α for convenience Note that this is an Initial-Boundary Value Problem:
◮ We impose an initial condition u(0, x) = u0(x) ◮ We impose boundary conditions on both sides of the domain
SLIDE 6 The Heat Equation
A natural idea would be to discretize uxx with a central difference, and employ the Euler method in time: Un+1
j
− Un
j
∆t − Un
j−1 − 2Un j + Un j+1
∆x2 = 0 Or we could use backward Euler in time: Un+1
j
− Un
j
∆t − Un+1
j−1 − 2Un+1 j
+ Un+1
j+1
∆x2 = 0
SLIDE 7 The Heat Equation
Or we could do something “halfway in between”:
Un+1
j
− Un
j
∆t − 1 2 Un+1
j−1 − 2Un+1 j
+ Un+1
j+1
∆x2 − 1 2 Un
j−1 − 2Un j + Un j+1
∆x2 = 0
This is called the Crank–Nicolson method2 In fact, it is common to consider a 1-parameter “family” of methods that include all of the above: the θ-method
Un+1
j
− Un
j
∆t − θ Un+1
j−1 − 2Un+1 j
+ Un+1
j+1
∆x2 − (1 − θ)Un
j−1 − 2Un j + Un j+1
∆x2 = 0
where θ ∈ [0, 1]
2From a paper by Crank and Nicolson in 1947, note: “Nicolson” is not a
typo!
SLIDE 8 The Heat Equation
With the θ-method:
◮ θ = 0 =
⇒ Euler
◮ θ = 1 2 =
⇒ Crank–Nicolson
◮ θ = 1 =
⇒ backward Euler For the θ-method, we can
- 1. perform Fourier stability analysis
- 2. calculate the truncation error
SLIDE 9 The θ-Method: Stability
Fourier stability analysis: Set Un
j (k) = λ(k)neik(j∆x) to get
λ(k) = 1 − 4(1 − θ)µ sin2 1
2k∆x
2k∆x
Here we cannot get λ(k) > 1, hence only concern is λ(k) < −1 Let’s find conditions for stability, i.e. we want λ(k) ≥ −1: 1 − 4(1 − θ)µ sin2 1 2k∆x
1 2k∆x
SLIDE 10 The θ-Method: Stability
Or equivalently: 4µ(1 − 2θ) sin2 1 2k∆x
For θ ∈ [0.5, 1] this inequality is always satisfied, hence the θ-method is unconditionally stable (i.e. stable independent of µ) In the θ ∈ [0, 0.5) case, the “most unstable” Fourier mode is when k = π/∆x, since this maximizes the factor sin2 1
2k∆x
SLIDE 11 The θ-Method: Stability
Note that this corresponds to the highest frequency mode that can be represented on our grid, since with k = π/∆x we have eik(j∆x) = eπij = (eπi)j = (−1)j The k = π/∆x mode:
1 2 3 4 5 6 7 8 9 10 −2 −1.5 −1 −0.5 0.5 1 1.5 2
j eπij
SLIDE 12
The θ-Method: Stability
This “sawtooth” mode is stable (and hence all modes are stable) if 4µ(1 − 2θ) ≤ 2 ⇐ ⇒ µ ≤ 1 2(1 − 2θ), Hence for θ ∈ [0, 0.5), the θ-method is conditionally stable
SLIDE 13 The θ-Method: Stability
0.1 0.2 0.3 0.4 0.5 5 10 15 20 25 30 35 40 45
θ µ
For θ ∈ [0, 0.5), θ-method is stable if µ is in the “green region,” i.e. approaches unconditional stability as θ → 0.5
SLIDE 14 The θ-Method: Stability
Note that if we set θ to a value in [0, 0.5), then stability time-step restriction is quite severe: ∆t ≤
(∆x)2 2(1−2θ)
Contrast this to the hyperbolic case where we had ∆t ≤ ∆x
c
This is an indication that the system of ODEs that arise from spatially discretizing the heat equation are stiff
SLIDE 15 The θ-Method: Accuracy
The truncation error analysis is fairly involved, hence we just give the result:
T n
j
≡ un+1
j
− un
j
∆t − θ un+1
j−1 − 2un+1 j
+ un+1
j+1
∆x2 − (1 − θ)un
j−1 − 2un j + un j+1
∆x2 = [ut − uxx] + 1 2 − θ
12(∆x)2uxxxx
1 24(∆t)2uttt − 1 8(∆t)2uxxtt
1 12 1 2 − θ
6!(∆x)4uxxxxxx
The term ut − uxx in T n
j vanishes since u solves the PDE
SLIDE 16
The θ-Method: Accuracy
Key point: This is a first order method, unless θ = 1/2, in which case we get a second order method! θ-method gives us consistency (at least first order) and stability (assuming ∆t is chosen appropriately when θ ∈ [0, 1/2)) Hence, from Lax Equivalence Theorem, the method is convergent
SLIDE 17 The Heat Equation
Note that the heat equation models a diffusive process, hence it tends to smooth out discontinuities Python demo: Heat equation with discontinous initial condition
2 4 6 8 10 1 2 3 0.2 0.4 0.6 0.8 1 x t
This is very different to hyperbolic equations, e.g. the advection equation will just transport a discontinuity in u0
SLIDE 18
Elliptic PDEs
SLIDE 19
Elliptic PDEs
The canonical elliptic PDE is the Poisson equation In one-dimension, for x ∈ [a, b], this is −u′′(x) = f (x) with boundary conditions at x = a and x = b We have seen this problem already: Two-point boundary value problem! (Recall that Elliptic PDEs model steady-state behavior, there is no time-derivative)
SLIDE 20 Elliptic PDEs
In order to make this into a PDE, we need to consider more than
Let Ω ⊂ R2 denote our domain, then the Poisson equation for (x, y) ∈ Ω is uxx + uyy = f (x, y) This is generally written more succinctly as ∆u = f We again need to impose boundary conditions (Dirichlet, Neumann, or Robin) on ∂Ω (recall ∂Ω denotes boundary of Ω)
SLIDE 21 Elliptic PDEs
We will consider how to use a finite difference scheme to approximate this 2D Poisson equation First, we introduce a uniform grid to discretize Ω
0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
x y
SLIDE 22 Elliptic PDEs
Let h = ∆x = ∆y denote the grid spacing Then,
◮ xi = ih, i = 0, 1, 2 . . . , nx − 1, ◮ yj = jh, j = 0, 1, 2, . . . , ny − 1, ◮ Ui,j ≈ u(xi, yj)
Then, we need to be able to approximate uxx and uyy on this grid Natural idea: Use central difference approximation!
SLIDE 23 Elliptic PDEs
We have
uxx(xi, yj) = u(xi−1, yj) − 2u(xi, yj) + u(xi+1, yj) h2 + O(h2),
and
uyy(xi, yj) = u(xi, yj−1) − 2u(xi, yj) + u(xi, yj+1) h2 + O(h2),
so that
uxx(xi, yj) + uyy(xi, yj) = u(xi, yj−1) + u(xi−1, yj) − 4u(xi, yj) + u(xi+1, yj) + u(xi, yj+1) h2 + O(h2)
SLIDE 24
Elliptic PDEs
Hence we define our approximation to the Laplacian as Ui,j−1 + Ui−1,j − 4Ui,j + Ui+1,j + Ui,j+1 h2 This corresponds to a “5-point stencil”
SLIDE 25
Elliptic PDEs
As usual, we represent the numerical solution as a vector U ∈ Rnxny We want to construct a differentiation matrix D2 ∈ Rnxny×nxny that approximates the Laplacian Question: How many non-zero diagonals will D2 have? To construct D2, we need to be able to relate the entries of the vector U to the “2D grid-based values” Ui,j
SLIDE 26 Elliptic PDEs
Hence we need to number the nodes from 1 to nxny — we number nodes along the “bottom row” first, then second bottom row, etc Let G denote the mapping from the 2D indexing to the 1D
- indexing. From the above figure we have:
G(i, j; nx) = jnx + i, and hence UG(i,j;nx) = Ui,j
SLIDE 27 Elliptic PDEs
Let us focus on node (i, j) in our F.D. grid, this corresponds to entry G(i, j; nx) of U Due to the 5-point stencil, row G(i, j; nx) of D2 will only have non-zeros in columns G(i, j − 1; nx) = G(i, j; nx) − nx, (1) G(i − 1, j; nx) = G(i, j; nx) − 1, (2) G(i, j; nx) = G(i, j; nx), (3) G(i + 1, j; nx) = G(i, j; nx) + 1, (4) G(i, j + 1; nx) = G(i, j; nx) + nx (5)
◮ (2), (3), (4), give the same tridiagonal structure that we’re
used to from differentiation matrices in 1D domains
◮ (1), (5) give diagonals shifted by ±nx
SLIDE 28
Elliptic PDEs
For example, sparsity pattern of D2 when nx = ny = 6
SLIDE 29 Elliptic PDEs
Python demo: Solve the Poisson equation ∆u = − exp
- −(x − 0.25)2 − (y − 0.5)2
, for (x, y) ∈ Ω = [0, 1]2 with u = 0 on ∂Ω
x y 0.2 0.4 0.6 0.8 1 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 0.01 0.015 0.02 0.025 0.03 0.035 0.04 0.045 0.05 0.055 0.06
SLIDE 30
Nonlinear Equations and Optimization
SLIDE 31 Motivation: Nonlinear Equations
So far we have mostly focused on linear phenomena
◮ Interpolation leads to a linear system Vb = y (monomials) or
Ib = y (Lagrange polynomials)
◮ Linear least-squares leads to the normal equations
ATAb = ATy
◮ We saw examples of linear physical models (Ohm’s Law,
Hooke’s Law, Leontief equations) = ⇒ Ax = b
◮ F.D. discretization of a linear PDE leads to a linear algebraic
system AU = F
SLIDE 32 Motivation: Nonlinear Equations
Of course, nonlinear models also arise all the time
◮ Nonlinear least-squares, Gauss–Newton/Levenberg–Marquardt ◮ Countless nonlinear physical models in nature, e.g.
non-Hookean material models3
◮ F.D. discretization of a non-linear PDE leads to a nonlinear
algebraic system
3Important in modeling large deformations of solids
SLIDE 33
Motivation: Nonlinear Equations
Another example is computation of Gauss quadrature points/weights We know this is possible via roots of Legendre polynomials But we could also try to solve the nonlinear system of equations for {(x1, w1), (x2, w2), . . . , (xn, wn)}
SLIDE 34 Motivation: Nonlinear Equations
e.g. for n = 2, we need to find points/weights such that all polynomials of degree 3 are integrated exactly, hence w1 + w2 = 1
−1
1dx = 2 w1x1 + w2x2 = 1
−1
xdx = 0 w1x2
1 + w2x2 2
= 1
−1
x2dx = 2/3 w1x3
1 + w2x3 2
= 1
−1
x3dx = 0
SLIDE 35 Motivation: Nonlinear Equations
We usually write a nonlinear system of equations as F(x) = 0, where F : Rn → Rm We implicity absorb the “right-hand side” into F and seek a root
In this Unit we focus on the case m = n, m > n gives nonlinear least-squares
SLIDE 36
Motivation: Nonlinear Equations
We are very familiar with scalar (m = 1) nonlinear equations Simplest case is a quadratic equation ax2 + bx + c = 0 We can write down a closed form solution, the quadratic formula x = −b ± √ b2 − 4ac 2a
SLIDE 37
Motivation: Nonlinear Equations
In fact, there are also closed-form solutions for arbitrary cubic and quartic polynomials, due to Ferrari and Cardano (∼ 1540) Important mathematical result is that there is no general formula for solving fifth or higher order polynomial equations Hence, even for the simplest possible case (polynomials), the only hope is to employ an iterative algorithm An iterative method should converge in the limit n → ∞, and ideally yields an accurate approximation after few iterations
SLIDE 38
Motivation: Nonlinear Equations
There are many well-known iterative methods for nonlinear equations Probably the simplest is the bisection method for a scalar equation f (x) = 0, where f ∈ C[a, b] Look for a root in the interval [a, b] by bisecting based on sign of f
SLIDE 39 Motivation: Nonlinear Equations
#!/usr/bin/python from math import * # Function to consider def f(x): return x*x-4*sin(x) # Initial interval: assume f(a)<0 and f(b)>0 a=1 b=3 # Bisection search while b-a>1e-8: print a,b c=0.5*(b+a) if f(c)<0: a=c else: b=c print "# Root at",0.5*(a+b)
SLIDE 40 Motivation: Nonlinear Equations
1 1.5 2 2.5 3 −4 −2 2 4 6 8 10 1.932 1.933 1.934 1.935 −0.01 −0.005 0.005 0.01
Root in the interval [1.933716, 1.933777]
SLIDE 41 Motivation: Nonlinear Equations
Bisection is a robust root-finding method in 1D, but it does not generalize easily to Rn for n > 1 Also, bisection is a crude method in the sense that it makes no use
- f magnitude of f , only sign(f )
We will look at mathematical basis of alternative methods which generalize to Rn:
◮ Fixed-point iteration ◮ Newton’s method
SLIDE 42
Optimization
SLIDE 43 Motivation: Optimization
Another major topic in Scientific Computing is optimization Very important in science, engineering, industry, finance, economics, logistics,... Many engineering challenges can be formulated as optimization problems, e.g.:
◮ Design car body that maximizes downforce4 ◮ Design a bridge with minimum weight
4A major goal in racing car design
SLIDE 44 Motivation: Optimization
Of course, in practice, it is more realistic to consider optimization problems with constraints, e.g.:
◮ Design car body that maximizes downforce, subject to a
constraint on drag
◮ Design a bridge with minimum weight, subject to a constraint
SLIDE 45 Motivation: Optimization
Also, (constrained and unconstrained) optimization problems arise naturally in science Physics:
◮ many physical systems will naturally occupy a minimum
energy state
◮ if we can describe the energy of the system mathematically,
then we can find minimum energy state via optimization
SLIDE 46 Motivation: Optimization
Biology:
◮ recent efforts in Scientific Computing have sought to
understand biological phenomena quantitively via optimization
◮ computational optimization of, e.g. fish swimming or insect
flight, can reproduce behavior observed in nature
◮ this jells with the idea that evolution has been “optimizing”
- rganisms for millions of year
SLIDE 47
Motivation: Optimization
All these problems can be formulated as: Optimize (max. or min.) an objective function over a set of feasible choices, i.e. Given an objective function f : Rn → R and a set S ⊂ Rn, we seek x∗ ∈ S such that f (x∗) ≤ f (x), ∀x ∈ S (It suffices to consider only minimization, maximization is equivalent to minimizing −f ) S is the feasible set, usually defined by a set of equations and/or inequalities, which are the constraints If S = Rn, then the problem is unconstrained
SLIDE 48 Motivation: Optimization
The standard way to write an optimization problem is min
x∈S f (x) subject to g(x) = 0 and h(x) ≤ 0,
where f : Rn → R, g : Rn → Rm, h : Rn → Rp
SLIDE 49 Motivation: Optimization
For example, let x1 and x2 denote radius and height of a cylinder, respectively Minimize the surface area of a cylinder subject to a constraint on its volume5 (we will return to this example later) min
x f (x1, x2) = 2πx1(x1 + x2)
subject to g(x1, x2) = πx2
1x2 − V = 0
5Heath Example 6.2
SLIDE 50 Motivation: Optimization
If f , g and h are all affine, then the optimization problem is called a linear program (Here the term “program” has nothing to do with computer programming; instead it refers to logistics/planning) Affine if f (x) = Ax + b for a matrix A, i.e. linear plus a constant6 Linear programming may already be familiar Just need to check f (x) on vertices of the feasible region
6Recall that “affine” is not the same as ”linear”, i.e.
f (x + y) = Ax + Ay + b and f (x) + f (y) = Ax + Ay + 2b
SLIDE 51 Motivation: Optimization
If the objective function or any of the constraints are nonlinear then we have a nonlinear optimization problem or nonlinear program We will consider several different approaches to nonlinear
Optimization routines typically use local information about a function to iteratively approach a local minimum
SLIDE 52 Motivation: Optimization
In some cases this easily gives a global minimum
−1 −0.5 0.5 1 0.5 1 1.5 2 2.5 3
SLIDE 53 Motivation: Optimization
But in general, global optimization can be very difficult
0.2 0.4 0.6 0.8 1 −0.1 −0.05 0.05 0.1 0.15 0.2 0.25 0.3 0.35
We can get “stuck” in local minima!
SLIDE 54 Motivation: Optimization
And can get much harder in higher spatial dimensions
0.2 0.4 0.6 0.8 1 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 −0.5 0.5 1 1.5 2 2.5
SLIDE 55 Motivation: Optimization
There are robust methods for finding local minimima, and this is what we focus on in AM205 Global optimization is very important in practice, but in general there is no way to guarantee that we will find a global minimum Global optimization basically relies on heuristics:
◮ try several different starting guesses (“multistart” methods) ◮ simulated annealing ◮ genetic methods7
7Simulated annealing and genetic methods are covered in AM207
SLIDE 56
Root Finding: Scalar Case
SLIDE 57 Fixed-Point Iteration
Suppose we define an iteration xk+1 = g(xk) (∗) e.g. recall Heron’s Method from Assignment 0 for finding √a: xk+1 = 1 2
xk
2 (x + a/x)
SLIDE 58 Fixed-Point Iteration
Suppose α is such that g(α) = α, then we call α a fixed point of g For example, we see that √a is a fixed point of gheron since gheron(√a) = 1 2 √a + a/√a
A fixed-point iteration terminates once a fixed point is reached, since if g(xk) = xk then we get xk+1 = xk Also, if xk+1 = g(xk) converges as k → ∞, it must converge to a fixed point: Let α ≡ limk→∞ xk, then8 α = lim
k→∞ xk+1 = lim k→∞ g(xk) = g
k→∞ xk
8Third equality requires g to be continuous
SLIDE 59
Fixed-Point Iteration
Hence, for example, we know if Heron’s method converges, it will converge to √a It would be very helpful to know when we can guarantee that a fixed-point iteration will converge Recall that g satisfies a Lipschitz condition in an interval [a, b] if ∃L ∈ R>0 such that |g(x) − g(y)| ≤ L|x − y|, ∀x, y ∈ [a, b] g is called a contraction if L < 1
SLIDE 60 Fixed-Point Iteration
Theorem: Suppose that g(α) = α and that g is a contraction
- n [α − A, α + A]. Suppose also that |x0 − α| ≤ A. Then the
fixed point iteration converges to α. Proof: |xk − α| = |g(xk−1) − g(α)| ≤ L|xk−1 − α|, which implies |xk − α| ≤ Lk|x0 − α| and, since L < 1, |xk − α| → 0 as k → ∞. (Note that |x0 − α| ≤ A implies that all iterates are in [α − A, α + A].) (This proof also shows that error decreases by factor of L each iteration)